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Moisture and density (MAD) measured on IODP Hole 347-M0061B
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Moisture and density (MAD) measured on IODP Hole 347-M0061A
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Moisture and density (MAD) measured on IODP Hole 347-M0060B
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Moisture and density (MAD) measured on IODP Hole 347-M0060A
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Moisture and density (MAD) measured on IODP Hole 347-M0059E
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Moisture and density (MAD) measured on IODP Hole 347-M0059D
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Moisture and density (MAD) measured on IODP Hole 347-M0059C
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Moisture and density (MAD) measured on IODP Hole 347-M0059B
This dataset has no description
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Moisture and density (MAD) measured on IODP Hole 347-M0059A
This dataset has no description
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Moisture and density (MAD) measured on IODP Hole 335-U1256D
Geocode = Depth CSF-A (m) -
(Table 1) Electrical resistivity, sound velocity, thermal conductivity, densi...
At Deep Sea Drilling Project (DSDP) Site 462, from mudline to 447 meters below the sea floor, Cenozoic nannofossil oozes and chalks have acoustic anisotropies such that... -
(Table 1) Physical properties at DSDP Hole 72-516F
Forty indurated sediment samples from Site 516 were studied to determine the cause of acoustic anisotropy in carbonate- bearing deep-sea sediments. Recovered from sub-bottom... -
(Table 1) Sediment characteristics at DSDP Hole 75-532A
Orientation and geometry of pores as well as sediment compressibility can be approximated by determining the shrinkage behavior of standardized samples. The sections... -
(Table 1) Physical properties of sediments at DSDP Holes 79-545 and 79-547A
Laboratory measurements of the acoustic and physical properties of deep-sea sediments and rocks are important for the interpretation of seismic reflection and refraction data... -
(Table 1) Comparisons of dynamic and static Young's moduli of basalt at DSDP ...
Compressional- and shear-wave velocity logs (Vp and Vs, respectively) that were run to a sub-basement depth of 1013 m (1287.5 m sub-bottom) in Hole 504B suggest the presence of... -
(Table 1) Porosity, particle diameter, ATP content and carbon and nitrogen co...
Sediment samples were obtained for detailed Adenosine 5'-Triphosphate (ATP) analysis down to 57.8 m below the seafloor (mbsf). The samples were also analyzed for particle-size... -
(Table 1) Physical properties of sediments at DSDP Leg 86 Holes
A wide variety of sediment types (red clays, carbonate oozes, and siliceous clays) were cored using the hydraulic piston corer on Leg 86 of the Deep Sea Drilling Project in the... -
(Table T1) Physical properties of minicores from ODP Leg 193 sites, PACMANUS ...
Permeability of the ocean crust is one of the most crucial parameters for constraining submarine fluid flow systems. Active hydrothermal fields are dynamic areas where fluid... -
Petrologic description and values of resistivity, CEC, and porosity of sample...
The resistivity, porosity, and cation exchange capacity of 36 basaltic samples recovered in Hole 504B during four DSDP and ODP legs have been measured in the laboratory at room... -
Processed physical properties measured on sediment core PS128_47-1
Sound knowledge about the petrophysical characteristics of a sediment core is a prerequisite for any subsequent paleoenvironmental study relying on sediment proxies. Physical...
